{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361981469178998784.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/95gb01070"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F95GB01070"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/95GB01070"}},{"identifier":{"@type":"NAID","@value":"30013378516"}}],"dc:title":[{"@value":"Production and dissolution of biogenic silica in the ocean: Revised global estimates, comparison with regional data and relationship to biogenic sedimentation"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We estimate the global rate of biogenic silica production in the ocean to be between 200 and 280 × 10<jats:sup>12</jats:sup> mol Si yr<jats:sup>−1</jats:sup>. The upper limit is derived from information on the primary productivity of the oceans, the relative contribution of diatoms to primary production and diatom Si/C ratios. The lower limit is derived independently using a multi‐compartment model of nutrient transport and biogenic particle flux, and field data on the balance between silica production and dissolution in the upper ocean. Our upper limit is 30–50% lower than several previous estimates, due to new data indicating lower values for both the relative contribution of diatoms to primary productivity and their Si/C ratios. Globally, at least 50% of the silica produced by diatoms in the euphotic zone dissolves in the upper 100 m, resulting in an estimated export of 100–140 × 10<jats:sup>12</jats:sup> mol Si yr<jats:sup>−l</jats:sup> to the deep ocean. Our estimates correspond to a global mean rate of biogenic silica production between 0.6 and 0.8 mol Si m<jats:sup>−2</jats:sup> yr<jats:sup>−1</jats:sup>. Incubation experiments indicate that silica production rates exceed that mean by a factor of 3–12 in coastal areas and are 2–4 times less than the global average in the oligotrophic mid‐ocean gyres. The mean silica production rate in waters overlying diatomaceous sediments (approximately 10–12% of the surface area of the oceans) is 0.7–1.2 mol Si m<jats:sup>−2</jats:sup> yr<jats:sup>−1</jats:sup>. That rate is only slightly higher than the global average, indicating that the silica produced in those regions is only 10–25% of the global total. The estimated production of biogenic silica in surface waters of the mid‐ocean gyres is approximately equal to that for all major areas of opal sediment accumulation combined. Regional comparison of silica production and accumulation rates suggests a strongly bimodal character in the efficiency of opal preservation in the sea. In waters overlying diatom‐rich sediments 15–25% of the silica produced in the surface layer accumulates in the seabed, while virtually none of the silica produced in other areas is preserved. The global burial/production ratio of ˜ 3% is a composite of those two very different systems. The mechanisms leading to more efficient opal preservation in regions of silica accumulation are presently unknown, but they have no simple relationship to primary productivity. Regional differences in opal preservation appear to be controlled by factors such as low surface temperature, selective grazing and aggregate formation, which diminish the rate of silica dissolution in surface waters and/or accelerate its transport to the seafloor.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469178998788","@type":"Researcher","foaf:name":[{"@value":"David M. Nelson"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469178998785","@type":"Researcher","foaf:name":[{"@value":"Paul Tréguer"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469178998787","@type":"Researcher","foaf:name":[{"@value":"Mark A. Brzezinski"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469178998784","@type":"Researcher","foaf:name":[{"@value":"Aude Leynaert"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469178998786","@type":"Researcher","foaf:name":[{"@value":"Bernard Quéguiner"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08866236"},{"@type":"EISSN","@value":"19449224"}],"prism:publicationName":[{"@value":"Global Biogeochemical Cycles"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1995-09","prism:volume":"9","prism:number":"3","prism:startingPage":"359","prism:endingPage":"372"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F95GB01070"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/95GB01070"}],"createdAt":"2004-02-04","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001201687097344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"Characterization of marine diatom-infecting virus promoters in the model diatom Phaeodactylum tricornutum"}]},{"@id":"https://cir.nii.ac.jp/crid/1050003824926010880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Super typhoon induced high silica export from Arakawa River, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050018816307314304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Transcriptional responses of the marine diatom Chaetoceros tenuissimus to phosphate deficiency"}]},{"@id":"https://cir.nii.ac.jp/crid/1050021072401573504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Nuclear Transformation of the Marine Pennate Diatom Nitzschia sp. 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Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412891868174592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Metabolomics-based approach to explore growth phase-dependent markers in cultured diatom Chaetoceros tenuissimus"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288083325312","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"珪藻のバイオファクトリー化を目指した基盤技術の開発"},{"@language":"en","@value":"Development of Basic Technologies for Biofactory Utilizing Diatoms"},{"@value":"珪藻のバイオファクトリー化を目指した基盤技術の開発 : 珪藻バイオファクトリー"},{"@language":"ja-Kana","@value":"ケイソウ ノ バイオファクトリーカ オ メザシタ キバン ギジュツ ノ カイハツ : ケイソウ バイオファクトリー"}]},{"@id":"https://cir.nii.ac.jp/crid/1390003825184234112","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Environmental and seasonal dynamics altering the primary productivity in Bingo-Nada (Bingo Sound) of the Seto Inland Sea, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390007381131963648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dietary analysis of bivalve larvae based on observation of the stomach contents using a scanning electron microscope"},{"@language":"ja","@value":"消化管内容物の走査型電子顕微鏡観察に基づく二枚貝浮遊幼生の食性解析"},{"@language":"ja-Kana","@value":"ショウカカン ナイヨウブツ ノ ソウサガタ デンシ ケンビキョウ カンサツ ニ モトズク ニマイガイ フユウヨウセイ ノ ショクセイ カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390021868461931264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seasonal changes in <i>Skeletonema</i> species in the sediment of Tokyo Bay evaluated with real-time PCR assays"},{"@value":"Seasonal changes in Skeletonema species in the sediment of Tokyo Bay evaluated with real-time PCR 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